Equidistant Conic Projection

A conic projection with equally spaced parallels. Neither conformal
nor equal area. Also known as the Simple Conic or Conic projection.

Scale

True along each meridian and along one or two chosen standard parallels,
usually but not necessarily on the same side of the Equator. As a rule
of thumb, these parallels can be placed at one-sixth and five-sixths of
the range of latitudes, but there are more refined means of selection.

Scale is constant along any given parallel.

Distortion

Free of angular and scale distortion only along the one or two standard
parallels. Distortion is constant along any given parallel. Compromise
in distortion between equal-area and conformal conic projections.

Usage

The most common projection in atlases for small countries. Also used
by the Soviet Union for mapping that nation.

Limitations

Use only for a single hemisphere.

Origin

Rudimentary forms developed by Claudius Ptolemy (about A.D. 100). Improvements
by Johannes Ryusch in 1508;, Gerardus Mercator in the late 16th century,
and Nicholas de l’Isle in 1745.

Limiting Forms

Polar Azimuthal Equidistant projection: if a pole is made the single
standard parallel. The cone of projection thereby becomes a plane.

Plate Carree projection: if the Equator is the single standard parallel.
The cone of projection thereby becomes a cylinder.

Equirectangular (Cylindrical) projection:
if the two standard parallels are symmetrically placed north and south
of the Equator.

Options

Specify the first standard parallel and second standard parallel to
tailor the projection to the area to be mapped.

Specify the latitude origin and longitude origin to center the map projection
to the area to be mapped. Specifying a non-Equatorial origin causes an
oblique projection.